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US3828245A Expired / Lapsed US ⏱️ 0.0 years remaining

Method of mapping bedding interfaces in a permafrost zone of an earth formation by electromagnetic radiation

Assignee: Chevron USA Inc
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Filing: 1971-10-04
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Granted: 1974-08-06
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Expires: 1991-10-04
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Abstract

Abstract A method for accurately and quickly mapping the location of bedding interfaces in the permafrost zone of an earth formation from a movable vehicle, say an aircraft, by transmitting electromagnetic radiation through the permafrost zone from a known geographic position on or above the permafrost''s surface, detecting a portion of energy reflected from each bedding interface of the permafrost zone and recording the two-way travel time of the energy reflected from each of the bedding interfaces so as to indicate distance - and hence location - of each bedding interface with respect to the known location of the electromagnetic radiation system.

Inventors

  • 👤 R Unterberger

Bibliographic Details

Application Number —
Jurisdiction US
Data Source google_patents
Last Synchronized 2026-10-27 22:08
CPC Classifications
G; G01; G01V; G01V3/00; G01V3/15; G01V3/17

Claims Analysis

Total Claims: 3
Claim 1
Independent Claim 272 words
Method of mapping bedding interfaces of different earth materials within a permafrost Zone of an earth formation by means of an electromagnetic generating and receiving means located at a known geographical location adjacent to the upper surface of said permafrost zone, which comprises: a. irradiating said permafrost zone with electromagnetic energy within a frequency range of 106 to 1011 Hertz by actuation of said electromagnetic generating and receiving means, b. detecting reflections of the electromagnetic energy from at least two interfaces within said permafrost zone, said interfaces forming electromagnetic discontinuities within said permafrost zone, said at least one interface being associated with the upper surface of said permafrost zone, said other interface being associated with the bottom of said permafrost zone, said reflections occurring because of different dielectric constants of said interfaces, c. also detecting reflections from electromagnetic discontinuities in a nonporous, nonfrozen zone immediately beneath said permafrost zone above a selected threshold value, d. recording the time for said electromagnetic energy to travel from substantially said upper and bottom surfaces, respectively, of said permafrost zone as well as from said discontinuities in said nonporous zone so as to provide a map which delineates the locations, depthwise, of said interfaces and said discontinuities within said permafrost and nonporous zones, respectively, e. interpreting the resulting record based on the difference in arrival times of reflection signals indicative of at least the location of the bottom of the permafrost zone and of the later arriving reflection signals of less magnitude, so as to indicate the locations of interfaces within the nonporous, nonfrozen zone beneath the permafrost zone favorable to the accumulation of hydrocarbons thereabout.
Claim 2
Dependent Claim 272 words
Method of mapping bedding interfaces of different earth materials within a permafrost Zone of an earth formation by means of an electromagnetic generating and receiving means located at a known geographical location adjacent to the upper surface of said permafrost zone, which comprises: a. irradiating said permafrost zone with electromagnetic energy within a frequency range of 106 to 1011 Hertz by actuation of said electromagnetic generating and receiving means, b. detecting reflections of the electromagnetic energy from at least two interfaces within said permafrost zone, said interfaces forming electromagnetic discontinuities within said permafrost zone, said at least one interface being associated with the upper surface of said permafrost zone, said other interface being associated with the bottom of said permafrost zone, said reflections occurring because of different dielectric constants of said interfaces, c. also detecting reflections from electromagnetic discontinuities in a nonporous, nonfrozen zone immediately beneath said permafrost zone above a selected threshold value, d. recording the time for said electromagnetic energy to travel from substantially said upper and bottom surfaces, respectively, of said permafrost zone as well as from said discontinuities in said nonporous zone so as to provide a map which delineates the locations, depthwise, of said interfaces and said discontinuities within said permafrost and nonporous zones, respectively, e. interpreting the resulting record based on the difference in arrival times of reflection signals indicative of at least the location of the bottom of the permafrost zone and of the later arriving reflection signals of less magnitude, so as to indicate the locations of interfaces within the nonporous, nonfrozen zone beneath the permafrost zone favorable to the accumulation of hydrocarbons thereabout.
Claim 3
Dependent Claim 54 words
The method in accordance with claim 1 in which said zone of nonporous, nonfrozen material is entrained with hydrocarbons to the extent that the resulting dielectric constant of said nonporous zone is at least 2.17 normalized to a room temperaature of 25* C and to a measuring frequency of about 300 X 106 Hertz.

References Cited (Backward Citations)

US2139460A Cited
US2426918A Cited
US2659882A Cited
US2657380A Cited
US3286163A Cited

USPTO Annuity & Maintenance Windows

Annuity Stage Window Opens Payment Deadline Surcharge Period Until Estimated Fee Status
3.5 Years (Year 4) 1977-08-05 1978-02-04 1978-08-06 $2000.00 Window Closed / Lapsed
7.5 Years (Year 8) 1981-08-05 1982-02-04 1982-08-06 $3760.00 Window Closed / Lapsed
11.5 Years (Year 12) 1985-08-05 1986-02-04 1986-08-06 $7700.00 Window Closed / Lapsed

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